Dissolved oxygen and O(2) flux across the water-air interface of the Changjiang Estuary in May 2003

CORC > 烟台海岸带研究所 > 中国科学院烟台海岸带研究所 > 中科院海岸带环境过程与生态修复重点实验室

	Dissolved oxygen and O(2) flux across the water-air interface of the Changjiang Estuary in May 2003
	Gao, Xuelu1,2 ; Song, Jinming 1
刊名	JOURNAL OF MARINE SYSTEMS
	2008-11-01
卷号	74 期号:1-2 页码:343-350
关键词	Dissolved oxygen Spatio-temporal distribution Oxygen flux Changjiang Estuary
英文摘要	The field observation of this study was carried out in the Changjiang Estuary from May 19 to 26,2003, just a few days before the Three Gorges Dam began to store water. A total of 29 stations, including 2 anchor stations, were distributed through almost the whole salinity gradient Based on the data gained from these stations, the biogeochemical characteristics of dissolved oxygen (DO) were examined. Spatial distribution of DO concentrations showed the pattern that it increased in a downriver direction. DO concentration generally varied within a narrow range of 733-8.10 mg l(-1) in the freshwater region and the west part of the mixed water region, and after that it increased rapidly. In vertical direction, the differences in DO concentrations between surface and 2 m above the bottom were big at the stations with water depths exceeding 20 m; DO concentration up to 14.88 mg l(-1) was recorded at the sea surface, while at 2 m above the bottom its concentration was only about 4 mg l(-1). The fluctuation in DO concentrations was small during a period of 48 h in the mixed water region and 2 m above the bottom of the seawater region; while it was large during the same period in the seawater region for surface and 5 m below the surface layer, and a maximum variation from 8.77 to 12.66 mg l(-1) in 4 h was recorded. Oxygen fluxes also showed a marked spatio-temporal variation. As a whole, the freshwater region and mixed water region were an oxygen sink while the seawater region was a source. Relationships between dissolved oxygen and some biogeochemical parameters which could markedly influence its spatio-temporal distribution were discussed in this paper. (C) 2008 Elsevier B.V. All rights reserved.
研究领域[WOS]	Geology ; Marine & Freshwater Biology ; Oceanography
关键词[WOS]	PAMLICO RIVER ESTUARY ; CARBON-DIOXIDE ; EUROPEAN ESTUARIES ; BOTTOM WATERS ; WIND-SPEED ; SEA ; EXCHANGE ; CO2 ; DEPLETION ; RESPONSES
收录类别	SCI
语种	英语
WOS记录号	WOS:000261256100019
公开日期	2016-04-26
内容类型	期刊论文
源URL	[http://ir.yic.ac.cn/handle/133337/9223]
专题	烟台海岸带研究所_中科院海岸带环境过程与生态修复重点实验室
作者单位	1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai 264003, Peoples R China
推荐引用方式 GB/T 7714	Gao, Xuelu,Song, Jinming. Dissolved oxygen and O(2) flux across the water-air interface of the Changjiang Estuary in May 2003[J]. JOURNAL OF MARINE SYSTEMS,2008,74(1-2):343-350.
APA	Gao, Xuelu,&Song, Jinming.(2008).Dissolved oxygen and O(2) flux across the water-air interface of the Changjiang Estuary in May 2003.JOURNAL OF MARINE SYSTEMS,74(1-2),343-350.
MLA	Gao, Xuelu,et al."Dissolved oxygen and O(2) flux across the water-air interface of the Changjiang Estuary in May 2003".JOURNAL OF MARINE SYSTEMS 74.1-2(2008):343-350.